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江汉平原中北部一次区域性暴雨的成因分析
An Analysis on Causes of a Torrential Rain in the Middle and North of Jianghan Plain
【摘要】 利用常规气象资料和NCEP再分析客观物理量场、卫星云图、多普勒雷达回波产品资料,对2007年7月13日发生在江汉平原中北部的暴雨过程进行了诊断分析。结果表明,(1)高空低槽东移是影响此次强降水过程的主要大尺度环流背景;(2)低层低涡暖切变和低空急流是暴雨的直接影响系统;(3)有利的热力水汽条件和动力条件是强降水产生和维持的机制;(4)卫星云图上"人"字型、"V"字型云系和多普勒速度资料上的"逆风区"、风切变可作为判断强降水落区落点的依据。
【Abstract】 Based on the conventional observations,satellite cloud images and Doppler radar data,a heavy precipitation process in the north of Jianghan Plain on 13 July 2007 is analyzed.The result shows that:(1) the low trough of upper air are the main large-scale circulation systems impacting this event;(2) the vortex and warm shear line of low-layer is the major systems;(3) the heat and water vapor conditions,and dynamic conditions are mechanism of the torrential rain;(4) cloud systems,upwind areas and shears can be used to judge the rainstorm areas.
【Key words】 vortex and shear line; cause of formation; precipitation area; diagnostic analysis;
- 【文献出处】 防灾科技学院学报 ,Journal of Institute of Disaster-Prevention Science and Technology , 编辑部邮箱 ,2008年03期
- 【分类号】P458.121.1
- 【被引频次】1
- 【下载频次】27